Soil is unique resource that most every living thing (above
deep water sources) relies on it for survival. Just like water is key part of
life. In the plant life, and health of atmosphere, Carbon intake is important
and the plants absorb Carbon and releases oxygen. Soil is a dynamic, living system that has sum
of carbon (C), which is an important regulator of the global carbon foot print.
Geological location on the planet, with climate and vegetation will influence
the Carbon (C) storage as will topography. Uplands can have a low amount of
Carbon (C) then low lands. In wet and hot climates increasing decomposing increase
the Carbon (C) in soil bank compared to dry and hot or cold that . Soil faunas,
roots, fungi, and microbes interact with mineral and organic material to
process the soil Carbon (C). Soil gasses are temperature sensitive and with
global warming occurring could release more C into the atmosphere. Carbon loss
in soil can also occur in erosion and leaching were dissolved carbon can be
present in groundwater. Carbon (C) storage can also be influence by the soil
texture which is based on particle size. Carbon in the soil is used by plants
along with CO2 in the atmosphere and in the respiration oxygen is
release. Many plant species form a reliance with certain fungi in the soil by
producing energy from their roots, like
carbon (C), and in return the fungi provides the plant with nutrients like
phosphorus..
Photo: The Natural Education
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